Kasuga Seamount
Kasuga 1
Stratovolkan · United States · 598 m (bawah laut)

- Tipe
- Stratovolkan
- Negara
- United States
- Wilayah
- Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
- Ketinggian
- 598 m (bawah laut)
- Koordinat
- 21.765, 143.710
- Letusan terakhir
- 1959
- Kondisi tektonik
- Subduction zone / Crustal thickness unknown
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
Kasuga 1, the northernmost of three seamounts in the the Kasuga seamount chain SE of Fukujin, rises from a depth of 3,000 m to within about 600 m of the ocean surface. A series of flank vents are located low on the southern side of the edifice. The summit does not have a caldera or display hydrothermal activity, and is largely covered by volcaniclastics. Altered basaltic and andesitic rocks dredged from the summit suggest that it is the oldest of the three seamounts, although delicately preserved lava flow lobes and toes from a flank eruption suggest a very youthful age. It is listed as an active volcano by the Japan Meteorological Agency, and floating pumice attributed to a submarine eruption was seen south of it in the summer of 1959. Water discoloration from a possible submarine eruption was reported near the seamount in November 1975.
Ringkasan Wikipedia
Ringkasan InggrisKasuga 1 is a seamount and active volcano of the Mariana volcanic arc. It rises 3,000 m (9,800 ft) above the seafloor to about 600 m (2,000 ft) beneath the ocean surface. The volcano represents the northernmost of the three that forms the Kasuga seamount chain and is located southeast of Fukujin. Its last confirmed eruption was in July 1959 which produced pumice and another possible eruption may have occurred in 1975 when discolored water was observed around the seamount. Based on the samples of basalt and andesite collected at the summit, it is the oldest of the seamounts.
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Riwayat letusan
Garis waktu rinci
- 1975VEI 0Perkiraan geologi1975-11-16 – Berlangsung21.78 N 143.71 E
- 1959VEI 0Teramati1959-07-15 – Berlangsung
Tautan eksternal
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